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Restoration of Floodplain Habitats for Inanga (Galaxias Maculatus) in the Kaituna River, North Island, New Zealand

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Restoration of Floodplain Habitats for Inanga (Galaxias Maculatus) in the Kaituna River, North Island, New Zealand View metadata, citation and similar papers at core.ac.uk brought to you by CORE Available online at www.science.canterbury.ac.nz/nznsprovided by UC Research Repository Restoration of floodplain habitats for inanga (Galaxias maculatus) in the Kaituna River, North Island, New Zealand Peter M. Ellery & Brendan J. Hicks* Centre for Biodiversity and Ecology Research, Department of Biological Sci- ences, School of Science and Engineering, The University of Waikato, Private Bag 3105, Hamilton 3240, New Zealand. *Corresponding author’s e-mail: [email protected] (Received 31 July 2008, revised and accepted 23 March 2009) Abstract The Kaituna River on New Zealand’s east coast is about 50 km long and drains lakes Rotorua and Rotoiti. An extensive flood control scheme, including stop-banks and gates, prevents flow of water from the lower river main channel to the original floodplain. In addition, a new, shortened channel (the Kaituna Cut) diverts the river directly to the sea instead of flowing through its original course into the Maketu Estuary. Minnow-trapping of inanga, common smelt, and bullies in 50 year-old ponds, recently constructed ponds, and riverine sites showed that new ponds were colonised by inanga within three months of construction. New ponds had higher catch rates than old ponds, and both new and old ponds had higher catch rates than the river, where no inanga were caught. Extrapolations from trap catch rates (2-13 inanga per 100 m2), suggest that old ponds held about 8-20 inanga per 100 m2, while in new ponds there were 24-67 inanga per 100 m2. Our study suggests that constructed ponds can provide suitable habitat for inanga from the Kaituna River to rear to adulthood, and shows the importance of off-river habitat for New Zealand’s most important whitebait species. Keywords: inanga – Galaxias maculatus – habitat restoration – artificial ponds. Introduction fish (Waters & Burridge 1999). Their diadromous juvenile stage (whitebait) Inanga, Galaxias maculatus (Jenyns 1842) enters New Zealand rivers principally is a globally widespread freshwater fish in spring (September to November). that is native to New Zealand, south- Whitebait runs in New Zealand have eastern Australia, South America and the declined in the last 40 years, and inanga Falkland Islands (McDowall 1990). The comprise most of the run in many rivers species has been characterised as one of (McDowall 1990). A combination of the world’s most widespread freshwater wetland drainage and flood control New Zealand Natural Sciences (2009) 34: 39-48. © New Zealand Natural Sciences 40 New Zealand Natural Sciences 34 (2009) schemes have isolated inanga from their course into the Maketu Estuary directly lowland rearing habitats, and are likely to the sea via a new, shortened channel at to have played some part in their decline. Te Tumu known as the Kaituna Cut (Fig- The Kaituna River on the east coast ure 1). Little floodplain remains within of New Zealand is about 50 km long the stop banks of the lower Kaituna River, and drains lakes Rotorua and Rotoiti. It and various flood control measures have has been subjected to an extensive flood resulted in 67 km of stop-bank, 88 km control scheme that involves stop-banks of canals and drains, seven pump stations and gates to prevent flow of water from and five flood gate structures (Goodhue the main river channel to the original 2007). Since settlement in 1880, exten- floodplain. In addition, the entrance of sive wetlands such as the Kaituna Swamp, the river was diverted from its original the Waihi Swamp, and the Kaawa Swamp Figure 1. Location of the Kaituna River and study ponds in the North Island, New Zealand. Source: Goodhue (2007). ELLERY & HICKS: Restoration of floodplain habitats for inanga 41 have been reduced to 248 ha, or less than < 0.1 m s-1 (Jowett 2002). Overhanging 1 % of the original wetland (Ministry for vegetation and other forms of cover fur- the Environment 1997). The Kaituna ther enhance inanga habitat (Richardson River catchment covers 124,000 ha, with & Taylor 2002). Density dependent 48 % of this below the Lake Rotoiti mechanisms appear to be more important outlet at Okere Falls. After falling 260 m than recruitment for determining inanga through a steep narrow gorge, the lower abundance in their study stream (Jowett river watershed of the Te Puke Lowlands & Richardson 2003). includes the Mangorewa River, Waiari Constructed ponds have been a focus and Ohineangaanga Streams and Rapa- of recent inanga habitat restoration, e.g., rahoe and Kopuroa canals. Mean annual in the Te Wae Wae Lagoon area, South discharge of the Kaituna River at the sea Island (Smith 2004), and on the Waiau is 49 m3 s-1. River floodplain (Paterson & Goldsmith In 1990, spawning grounds for the 2002). Traps have been used to evaluate most common whitebait species, inanga the success of habitat restoration, and (Galaxias maculatus), were identified opinions have varied on the dependence on the lower Kaituna River. Generally, of catch rate on various types of bait (e.g., inanga are known to spawn within 1 Millar 2001, McDonald 2007). Few km of the upstream end of the saltwater evaluations of the effect of baiting have wedge (Mitchell 1990). In the Kaituna been carried out. River, inanga have been observed spawn- The objectives of this study were to ing on both banks about 2 km upstream evaluate the influence of bait on inanga from the sea in and around the location catch rates, to excavate new ponds next of the old ponds (the Borrow Pits) in to existing ponds on a small apron of 1988, 1989, and 1990 (Mitchell 1990). floodplain, to compare inanga catch Rearing inanga require low water veloci- rates in ponds and riverine sites, and to ties, avoiding velocities > 0.2 m s-1, but compare recruitment of inanga to newly have broad requirements for substrate constructed and older ponds as the mi- and water depth > 0.25 m (Lamouroux gration and rearing season progressed & Jowett 2005). Feeding velocities are (October to February). Table 1. Water depths at high and low tides and approximate pond dimensions. Pond areas exclude the areas occupied by islands (30% of FNP, 25% of ENP, and 10% of LNP). Site name Site type Code N traps Depth (m) Pond dimensions Width Length Area High tide Low tide (m) (m) (m2) River site River RS 10 1.5 - 2.2 0.4 Estuary pond Old pond EP 0 1.1 - 1.8 0 11 44 490 Small pond Old pond SP 5 1.3 - 2.0 0.2 11 29 250 Feeder channel Old pond FC 15 1.3 - 2.0 0.2 11 167 1830 First new pond New pond FNP 6 1.7 - 2.4 0.6 22 29 360 East new pond New pond ENP 6 1.6 - 2.3 0.5 27 36 560 Long new pond New pond LNP 8 1.6 - 2.3 0.5 22 84 1330 Total 50 42 New Zealand Natural Sciences 34 (2009) Table 2. The influence of different baits on catch rates of inanga, common smelt, and bullies in artificial ponds in the lower Kaituna River floodplain between 29 June and 15 July 2007. Bait N traps Inanga Common smelt Bullies Mean SE Mean SE Mean SE Cheese 16 7.56 3.30 1.31 0.68 0.38 0.20 None 16 2.81 1.26 0.38 0.20 0.63 0.24 Cat biscuits 16 1.56 0.77 0.06 0.06 0.63 0.24 Vegemite 16 1.25 0.59 0.13 0.09 0.88 0.34 Methods herb Polygonum sp., and reed sweetgrass Glyceria maxima. Study site Between 2003 and 2006, the Maketu Before excavation of the new ponds, Taiapure fenced off the floodplain sur- inanga spawning habitat was identified rounding the ponds from grazing ani- in the outflows of ponds known locally mals, cleared gorse (Ulex europaeus), and as the Borrow Pits, located on the true planted some native vegetation. Three right of the Kaituna River (NZ map new ponds (First new pond, FNP; East grid 2809675E, 6377740N, latitude new pond, ENP; and Long new pond, 37.75175oS, longitude 176.39910oE; LNP) were constructed between 12 and Figure 1). These ponds were created by 14 June 2007, and the culvert between the excavation of material to form the EP and FC was removed (Figure 1). This flood protection stop-bank in the mid isolated the area to be excavated from the 1950s. The area of the Borrow Pits is river, giving the lowest possible water level contained in a loop of riverbank on the for the period of the work and containing river side of the flood protection stop- sediment produced by excavation within bank. No spawning was observed at the the Borrow Pits area. The pond areas in Borrow Pits in the autumns of 2000 and Table 1 exclude the areas occupied by 2001, but in autumn 2002, pre- and islands (30% of FNP, 25% of ENP, and post-spawning fish were trapped (Young 10% of LNP). More detail on pond con- & Ellery 2002). struction with photographs is provided in The old ponds are relatively long and Ellery (2008). narrow (Figure 1). Estuary Pond (EP) Bait comparison trial and the Feeder Channel (FC) pond run parallel to the stop-bank, and water in A trial was set up in SP at the upriver FC is fed only through EP through a end of the Borrow Pits using 6 mm mesh culvert. The Small Pond (SP) has its own Gee minnow traps. SP was not affected connection to the river. EP completely by the excavations.
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